The Native Sacramento Valley Red Fox ______
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TYPICAL VALLEY INDIAN HOMES Vol. 2 No. 11 YUBA CITY, CALIFORNIA
Vol. 2 No. 11 YUBA CITY, CALIFORNIA OCTOBER 17 1961 TYPICAL VALLEY INDIAN HOMES SUTTER COUNTY HISTORICAL SOCIETY FALL MEETING OCTOBER 17, 1961 TUESDAY EVENING — 8 P.M. PLACE: Board of Supervisors Chambers County Office Building, 2nd Street PRESIDENT: Mrs. Florence Arritt PROGRAM CHAIRMAN: Randolph Schnabel PROGRAM SPEAKER: Waddell F. Smith President, National Pony Express Centennial Association TOPIC: The History of the Pony Express and Its Centennial BOARD OF DIRECTORS MINUTES October 5, 1961 The Board of Directors of Sutter County Historical Society met in regular session October 5, 1961 at 7:30 P.M. in the office of the County Superintendent. The meeting was called to order by Vice President, Mrs. Ida Littlejohn in the absence of the president, Mrs. Florence Arritt. Mrs. Arritt is on her vacation traveling in the southwest and visiting many spots of historic interest such as Tombstone, Arizona. The minutes of the July Board meeting and regular meeting were read and approved. The treasurer reported cash in the bank $737.33. Film Fund $447.00 and general fund $290.33. Mr. Ramey reported a membership of 111. Fifteen new members were secured at the county fair booth. The following bills were approved for payment: Valley Print Shop — Membership Cards, Stationery $41.70. County of Sutter — Bulletin pictures $6.20. Earl Ramey — Postage $3.50. Program Chairman, Randolph Schnabel reported the program had already been arranged for the annual dinner meeting in January. Mrs. Gibson presented an invitation to the Sutter County Historical Society to en- tertain the Symposium of Historical Societies of Northern California and Southern Oregon in the fall of 1962. -
HYDROLOGY and WATER QUALITY 3.8 Hydrology and Water Quality
3.8 HYDROLOGY AND WATER QUALITY 3.8 Hydrology and Water Quality This section of the Draft EIR addresses the potential for the Merced General Plan to affect or modify the existing hydrology and water quality of the Planning Area. Two comment letters were received on the NOP from the Merced Irrigation District (MID) in which they said that they would “Upon development of new and existing land covered within the scope of the 2030 General Plan, MID will provide a detailed response in regards to the proposed projects and their impacts upon MID facilities.” The second letter received was in response to the NOP regarding hydrology and water quality. The commenter wants the City to prepare a Water Element and “perform an environmental review of the potentially positive environmental effects that could be based upon such additional elements.” 3.8.1 SETTING Environmental Setting CLIMATE The climate of the City of Merced is hot and dry in the summer and cool and humid in the winter. The average daily temperature ranges from 47 to 76 degrees Fahrenheit. Extreme low and high temperatures of 15°F and 111°F are also known to occur. Historical average precipitation is approximately 12” per year, with the rainy season commencing in October and running through April. On average, approximately 80% of the annual precipitation occurs between November and March. The hot and dry weather of the summer months usually results in high water demands for landscape irrigation during those months. REGIONAL TOPOGRAPHY The project area is located in and immediately adjacent to the City of Merced. -
Geologic Features and Ground-Water Storage Capacity of the Sacramento Valley California
Geologic Features and Ground-Water Storage Capacity of the Sacramento Valley California By F. H. OLMSTED and G. H. DAVIS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1497 Prepared in cooperation with the California Department of ff^ater Resources UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1961 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director Tlie TT.S. Geological Survey Library catalog card for this publication appears after page 241. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract___________________________________________________ -_ 1 Introduction.-.--- .___-___________-___._--.______-----_ 5 Purpose and scope of the investigation.__________________ ______ 5 Location of area__-__-________-____________-_-___-_-__--____-_- 6 Development of ground water___________________-___-__ ___ __ 7 Acknowledgments....-------- ____________ _________________ 8 Well-numbering system..________________________________ _ 9 Geology--__--_--_--__----_--_-----____----_ --_ ___-__-- 10 Geomorphology_____________________________________________ 10 General features _______________________________________ 10 Mountainous region east of the Sacramento Valley...__________ 11 Sierra Nevada_______________________________________ 11 Cascade Range.._____________________-__--_-__-_---- 13 Plains and foothill region on the east side of the Sacramento Valley..__-_________-_.-____.___________ 14 Dissected alluvial uplands west of the Sierra -
An Examination of a Barrier Jet in the Sacramento Valley Using the Weather Event Simulator (WES)
An Examination of a Barrier Jet in the Sacramento Valley Using the Weather Event Simulator (WES) James Mathews, WFO Sacramento, CA & John Juskie, WFO Sacramento, CA Introduction Barrier winds or barrier jets are common occurrences in the Sacramento valley due to the orientation of the topography. The Sacramento valley is bounded by the Sierra Nevada Mountains to the east and the coastal range to the west. These mountains often cause terrain-induced winds in the Sacramento valley. As an example, onshore flow from the Pacific Ocean causes air to be forced through the gap in the coastal range mountains called the Golden Gate. Once the air passes through the Carquinez Strait east of the Golden Gate, it spreads out as it reaches the valley and results in a southerly wind direction for the Sacramento valley. Usually, these wind speeds are not strong enough to cause significant problems. However, on occasion, southerly winds can result in the formation of the southerly barrier jet along side the Sierra Nevada Mountains (Parish, 1982). Given unique circumstances, wind speeds can become significant to the public and wind advisories, high wind warnings, or Red Flag Warnings are issued to highlight this phenomenon. Staudenmaier (1994) discussed the formation of a northerly barrier jet and the implications to extreme fire behavior. Staudenmaier offered three conditions forecasters should examine for the potential development of a northerly barrier jet: (1) a sufficiently deep surface or near-surface based layer (at least 150 mbs deep) of northeasterly flow over the Sacramento valley for at least 6 hours, (2) strong stability as shown by the Oakland, CA (KOAK) sounding extending from around 800 mbs to at least as high as the terrain and, (3) enhancement of gusty surface winds if the stable layer caps a slightly less stable layer allowing for momentum transfer to the surface. -
California's San Joaquin Valley: a Region and Its Children Under Stress
CALIFORNIA’S SAN JOAQUIN VALLEY: A REGION AND ITS CHILDREN UNDER STRESS January 2017 Commissioned by Study Conducted by California’s San Joaquin Valley: A Region and Its Children Under Stress January 2017 Dear Colleagues, We are pleased to share with you California’s San Joaquin Valley: A Region and its Children Under Stress, commissioned by the San Joaquin Valley Health Fund, with funding from the W.K. Kellogg Foundation and Sierra Health Foundation, and prepared by the UC Davis Center for Regional Change. In preparing this report, researchers met with residents and those working with and on behalf of Valley communities to learn what their priorities are for policy and systems change. As detailed in the report, their quest for a more equitable region is focused on several priorities that include early education, healthy food, healthy living environments and equitable land use planning as the primary issues of concern. While the report documents the many racial, health and other inequities, and the particular effects they have on the lives and life chances of families raising children in the region, it also presents the vision of local leaders and community residents. We know the challenges that lie ahead will be difficult to address. While the San Joaquin Valley includes the top agricultural producing counties in California, almost 400,000 of the region’s children live in poverty and seven of the 10 counties with the highest child poverty rates in the state are in the Valley. One out of every four Valley children experiences food insecurity and they are much more likely to be exposed to pesticides while in school and to go to schools with unsafe drinking water. -
San Joaquin Valley, California
SAN JOAQUIN VALLEY, CALIFORNIA Largest human alteration of the Earth’s surface CALIFORNIA ining ground water for agriculture has enabled the San Joaquin Valley of California to become one of the world’s most productive agricultural regions, while simulta- S a M c neously contributing to one of the single largest alterations of the r a m C land surface attributed to humankind. Today the San Joaquin Valley e n t o is the backbone of California’s modern and highly technological E R . S N . agricultural industry. California ranks as the largest agricultural R r I e h t producing state in the nation, producing 11 T E a e F R percent of the total U.S. agricultural value. R R A The Central Valley of California, which A L includes the San Joaquin Valley, the Sacra- Delta mento Valley, and the Sacramento-San N E Joaquin Delta, produces about 25 percent S V a n A of the nation’s table food on only 1 percent San Francisco Bay Jo a D q of the country’s farmland (Cone, 1997). u A in V R iver In 1970, when the last comprehensive sur- A Mendota L veys of land subsidence were made, sub- L sidence in excess of 1 foot had affected E more than 5,200 square miles of irrigable Y San Joaquin Valley P land—one-half the entire San Joaquin a c i Valley (Poland and others, 1975). The f i c maximum subsidence, near Mendota, was O c more than 28 feet. e a n 0 80 Miles 0 80 Kilometers Approximate location of maxi- mum subsidence in United States identified by research efforts of Joseph Poland (pic- tured). -
4.9 Biological Resources
METROPOLITAN BAKERSFIELD METROPOLITAN BAKERSFIELD GENERAL PLAN UPDATE EIR 4.9 BIOLOGICAL RESOURCES The purpose of this Section is to identify existing biological resources within the Metropolitan Bakersfield area. In addition, this Section provides an assessment of biological resources (including sensitive species) impacts that may result from implementation of the General Plan Update references General Plan goals and policies, and, where necessary, recommends mitigation measures to reduce the significance of impacts. This Section describes the biological character of the site in terms of vegetation, flora, wildlife, and wildlife habitats and analyzes the biological significance of the site in view of Federal, State and local laws and policies. ENVIRONMENTAL SETTING The study area for the Metropolitan Bakersfield General Plan Update encompasses 408 square miles of the southern portion of the San Joaquin Valley, the southernmost basin of the Central Valley of California. Prior to industrial, agricultural and urban development, the San Joaquin Valley comprised a variety of ecological communities. Runoff from the surrounding mountains fostered hardwood and riparian forests, marshes and grassland communities. Away from the influence of the mountain runoff, several distinct dryland communities of grasses and shrubs developed along gradients of rainfall, soil texture and soil alkalinity, providing a mosaic of habitats for the assemblage of endemic plants and animals. Agriculture, urban development and oil/gas extraction have resulted in many changes in the natural environment of the San Joaquin Valley. For example, lakes and wetlands in the delta area have been drained and diverted, native plant and animal species have been lost and a decrease in the acreage of native lands has occurred. -
About Kern County • Background Kern County • Water Use • Water Sources R.I
Water in Bakersfield and Kern County About Kern County • Background Kern County • Water use • Water sources R.I. Connecticut 1,212 sq. mi. • Entities that control water 5,018 sq. mi. • Groundwater recharge Delaware 2,045 sq. mi. Area 8,170 sq. mi. – Kern County covers 5.21 million Sources: acres, roughly the area of Tom Haslebacher, Kern County Water Agency Connecticut, Delaware and Rhode Jon Parker, Kern Water Bank Authority Island. About Kern County About Kern County Delano Kernville Area Ridgecrest McFarland About one-third of Inyokern Wasco Kern’s area is on Shafter the valley floor, Oildale BAKERSFIELD which is intensively Population Lamont cultivated. Kern County’s Arvin California City Taft There are 860,000 irrigated acres population is Tehachapi 677,400. It is one of on the valley floor, one-third of Maricopa which are permanent crops. the fastest growing counties in the state, Kern consistently ranks 3rd or 4th in growing 19% since the state in value of production. 1995, and about 2% per year. Kern is California’s 14th most populous county. Annual water usage in Kern County: Municipal and industrial - 182,000 acre-feet Agricultural - 2,250,000 acre-feet 1 Gross Water Supplies and Net Water Requirements San Joaquin Valley Portion of Kern County Acre-Feet July 5, 2001 4,500,000 4,000,000 Additions to Kern County water sources: 3,500,000 Groundwater Storage 3,000,000 Kern River - 22% 2,500,000 Withdrawals from 2,000,000 Groundwater Storage State Water Project (California Aqueduct) - 1,500,000 23% 1,000,000 500,000 Federal (Friant-Kern -
Birding Hotspots of the Northern Sacramento Valley 15 Miles North to Red Bluff ° Upper Bidwell Park !!# !!# 6 Duncan Wildwood !Hcorning ")2 East Ave
Birding Hotspots of the Northern Sacramento Valley 15 miles north to Red Bluff ° Upper Bidwell Park !!# !!# 6 Duncan Wildwood !HCorning ")2 East Ave. Manzanita MainSt Corning 3 ")1 Samuel Ayer/ ") Sacramento River NWR - Bruce Dog Island Park South Ave City Main St Rio Vista Unit ¤£99 Breckenridge of 32 ¤£ Bruce Rd City of Antelope Chico §¨¦I-5 ¤£32 Red £99 Skyway ° Dominic S ¤ S a River Rd. a c ° Bluff c r Morrow r ° a a Genetic Resource & m 11 m Conservation Center Cramer ee n County Rd 200 e tto k o R a R iiv L v ee r e r t t u County Rd 200 I-5 B §¨¦ Sacramento River NWR- k East Ave 6 k k c ")4 Pine Creek Unit ")Bruce Rd e e la Hamilton City ee B Orland ")5 ¤£32 CCrr !H tet e 32 t ¤£ !H t !H uu Black Butte Rd Chico BB ¤£99W ")7 W Sacramento Ave Chico ¤£45 10 11 ")8 ") ") Skyway ")9 Chico River Rd ")12 Oroville-Chico Hwy Sacramento River NWR- ¤£191 Ord Bend Unit River Rd Durham Dayton Hwy ¤£70 ")15 14 Rd 32 Road 33 ") Ord Ferry Road ")17 Grainland Rd ¤£149 Road R ")16 Table # # Llano Seco Unit - Midway !! !! Road WW Mountain ")13 Steve Thompson 18 Road 39 North Central Valley ") Wildlife Mg't Area ¤£99 ")19 Seven Mile Lane Cottonwood Rd. Upper Butte Nelson Rd £162 Basin WA - ")20 ¤ Llano Seco Unit !H ¤£162 Nelson Rd Willows Upper T Road V h 162 !H Aguas Frias Rd ¤£ Butte e Road WW r m Oroville Road 57 Road P Rd 57 Basin WA - Oroville Rd Rd W l Howard i National Wildlife Refuge Road 59 t Larkin Rd Slough Unit ")21 o 22 ¤£162 Af terbay ") Road 60 State Wildlife Area Road 61 !HButte City Oroville Hamilton WA Sacramento State Park 24 River NWR- ") Road Z 23 Packer Unit ") Afton Rd City Park Upper Afton Afton Blvd(RdY) Road 68 !H Butte Roads Sacramento PrincetonPrinceton Basin WA - NWR Little Dry Gravel Creek Unit Butler Rd Adobe Rd !H Gridley Colusa Hwy Gridley Paved Rd. -
San Joaquin Valley Groundwater Basin Kings Subbasin
Tulare Lake Hydrologic Region California’s Groundwater San Joaquin Valley Groundwater Basin Bulletin 118 San Joaquin Valley Groundwater Basin Kings Subbasin • Groundwater Subbasin Number: 5-22.08 • County: Fresno, Kings, and Tulare • Surface Area: 976,000 acres (1,530 square miles) Subbasin Boundaries and Hydrology The San Joaquin Valley is surrounded on the west by the Coast Ranges, on the south by the San Emigdio and Tehachapi Mountains, on the east by the Sierra Nevada and on the north by the Sacramento-San Joaquin Delta and Sacramento Valley. The northern portion of the San Joaquin Valley drains toward the Delta by the San Joaquin River and its tributaries, the Fresno, Merced, Tuolumne, and Stanislaus Rivers. The southern portion of the valley is internally drained by the Kings, Kaweah, Tule, and Kern Rivers that flow into the Tulare drainage basin including the beds of the former Tulare, Buena Vista, and Kern Lakes. The Kings Subbasin is bounded on the north by the San Joaquin River. The northwest corner of the subbasin is formed by the intersection of the east line of the Farmers Water District with the San Joaquin River. The west boundary of the Kings Subbasin is the eastern boundaries of the Delta- Mendota and Westside Subbasins. The southern boundary runs easterly along the northern boundary of the Empire West Side Irrigation District, the southern fork of the Kings River, the southern boundary of Laguna Irrigation District, the northern boundary of the Kings County Water District, the southern boundaries of Consolidated and Alta Irrigation Districts, and the western boundary of Stone Corral Irrigation District. -
Analysis of San Joaquin County Economic & Social Indicators
SJC Index San Joaquin County 2020 Analysis of San Joaquin County Economic & Social Indicators Prepared by: Meredith Huang, Jeremy Padge and Thomas E. Pogue 2 Forward This report is being released in fall 2020, a year defined by extreme social and economic change due to the global COVID‐19 pandemic. At this time, very few of the indicators highlighted in this report have any local, San Joaquin County, data available for 2020, and what is available covers only the very initial stages of the pandemic. As a result, we have decided to only present data indicators in this report through the end of 2019. In this sense, we believe it provides a useful snapshot of the current state and progress of San Joaquin County just prior to the onset of the COVID‐19 pandemic. As we review these indicators in the future, some social, economic, and demographic characteristics of the county described in these pages will return to pre‐pandemic trends while others may be fundamentally changed. Thus, this edition of the San Joaquin County Index can serve as a useful benchmark for measuring the effects of COVID‐19, and a picture of the County’s comparative profile without the confounding effects of COVID‐19 that have made many traditional data indicators difficult to interpret. By reviewing data indicators for San Joaquin County and its communities in comparison to the other counties, regions, the state and the nation, the Index fosters a shared understanding about opportunities and challenges. Thus, the Index provides a foundation of reliable information to support actions to advance economic and community development. -
Geochemistry of Ground Water in the 1 Sacramento Valley, California
IQJUN GEOCHEMISTRY OF GROUND WATER IN THE 1 SACRAMENTO VALLEY, CALIFORNIA U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1401-B Geochemistry of Ground Water in the Sacramento Valley, California By LAURENCE C. HULL CENTRAL VALLEY OF CALIFORNIA RASA PROJECT GEOLOGICAL SURVEY PROFESSIONAL PAPER 1401-B UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1984 UNITED STATES DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Hull, Laurence C. Geochemistry of ground water in the Sacramento Valley, California (Geological Survey Professional Paper 1401-B) (Central Valley of California RASA Project) Bibliography: 36 p. 1. Water, Underground California Sacramento Valley. 2. Water chemistry. I. Title. II. Series. III. Series: Central Valley of California RASA Project. GB1025.C2H781984 551.4'9'097945 84-600016 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract .................. Bl Temporal changes ............... B13 Introduction ................ 1 Methods of data analysis ........ 15 Geography ............... 1 Dissolved solids .............. 15 Purpose and scope .......... 3 Hydrochemical facies ......... 16 Data compilation ............ 3 1 Nitrate ................... 19 Well-numbering system ........ 3 Hydrochemical facies ......... 20 Acknowledgments ........... 3 Hypothesis testing ............ 21 Description of the study area ...... 3 Processes controlling ground-water chemistry 22 Geology and geomorphology ..... 3 Methods of data analysis ........ 22 Geologic synopsis ......... 4 Principal components analysis .... 22 Geomorphic units ......... 4 Trend surface analysis ........ 22 Hydrogeology ............. 6 Processes and their spatial variation . 22 Hydrochemical facies ........... 7 Mineral stability relations ........... 25 Criteria and procedure for division . 7 Mineralogy of sediments ......... 25 Descriptions of hydrochemical facies Well 12N/01E-34Q .......... 25 Tuscan volcanic rocks .....